The depth below the Earth's surface of the lithosphere varies depending on location, but on average it extends to about 100 kilometers (62 miles) deep. This layer includes the crust and upper part of the mantle and is characterized by its rigidity and brittle behavior.
The Gutenberg Discontinuity is found beneath the Mohorovičić discontinuity (Moho) in the lithosphere. It is located at a depth of about 70 km to 400 km below the Earth's surface. This boundary separates the upper mantle from the lower mantle.
The outer shell of Earth that extends to a depth of 100km is known as the lithosphere. It consists of the crust and the uppermost part of the mantle and is divided into tectonic plates that float on the semi-fluid asthenosphere below.
The boundary between the asthenosphere and the lithosphere is normally below the Moho (which marks the boundary between the crust and the mantle). The exception to this is below mid-ocean ridges where the moho and the lithosphere / asthenosphere boundary are at the same depth.
The softer layer below the lithosphere is the asthenosphere. The asthenosphere begins at a depth of approximately 150 km. It has convection currents that arise from the heating and subsequent rising of material from the lower asthenosphere. These convection currents drive the movement of lithospheric plates at the surface, and are the cause of tectonic activity.
The Moho, or Mohorovičić discontinuity, is typically found at a depth of about 5-70 kilometers (3-43 miles) below the Earth's surface. It marks the boundary between the Earth's crust and the underlying mantle.
The Earth's lithosphere can vary in depth from 5 km at the ocean ridges to 200 km underneath mountain ranges.
The asthenosphere is a region of Earth's upper mantle that is partially molten and flows slowly, allowing tectonic plates to move. It is located beneath the lithosphere and extends to a depth of about 200 kilometers below the surface.
temperature increases with depth
The Gutenberg Discontinuity is found beneath the Mohorovičić discontinuity (Moho) in the lithosphere. It is located at a depth of about 70 km to 400 km below the Earth's surface. This boundary separates the upper mantle from the lower mantle.
Earthquakes can occur at varying depths below the Earth's surface, typically ranging from near the surface to around 700 kilometers deep. The depth of an earthquake's focus can provide insight into the type of earthquake and the tectonic plate boundary where it occurred.
50km
The outer shell of Earth that extends to a depth of 100km is known as the lithosphere. It consists of the crust and the uppermost part of the mantle and is divided into tectonic plates that float on the semi-fluid asthenosphere below.
At a depth of 500 m below the surface, the pressure would be approximately 5 atmospheres (1 atm for every 10 m of depth).
The boundary between the asthenosphere and the lithosphere is normally below the Moho (which marks the boundary between the crust and the mantle). The exception to this is below mid-ocean ridges where the moho and the lithosphere / asthenosphere boundary are at the same depth.
The temperature of the lithosphere can vary depending on factors such as depth and location. Generally, the temperature increases with depth, with the top of the lithosphere being cooler than the lower parts. At the surface, temperatures can range from around 0°C in polar regions to over 50°C in hot desert areas.
The softer layer below the lithosphere is the asthenosphere. The asthenosphere begins at a depth of approximately 150 km. It has convection currents that arise from the heating and subsequent rising of material from the lower asthenosphere. These convection currents drive the movement of lithospheric plates at the surface, and are the cause of tectonic activity.
The pressure is greater at 20 m below the surface of the sea. Pressure increases with depth due to the weight of the water above. Each additional meter of depth adds more pressure, so the pressure will be higher at 20 m compared to 10 m below the surface.